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粤北石漠化灌丛坡地模拟降雨地表径流水中钙离子含量变化
引用本文:魏兴琥,陆冠尧,周红艳,徐喜珍,雷俐.粤北石漠化灌丛坡地模拟降雨地表径流水中钙离子含量变化[J].中国沙漠,2011,31(5):1343-1347.
作者姓名:魏兴琥  陆冠尧  周红艳  徐喜珍  雷俐
作者单位:1. 佛山科学技术学院国土资源环境与旅游研究中心,广东佛山,528000
2. 华南师范大学地理科学学院,广东广州,510630
基金项目:国家自然科学基金项目(30870469,31170486)资助
摘    要: 通过模拟降雨试验,研究粤北地区不同石漠化程度的灌丛坡地地表径流水中钙离子含量的变化。结果表明,在不同雨强下,不同石漠化灌丛坡地地表径流量、地表径流水钙离子浓度和地表径流水钙离子总量随石漠化程度的加重呈逐渐上升后又降低的倒“U”型趋势;在同一雨强下,潜在、轻度和极重度石漠化坡地径流水钙离子流失量远低于中度和重度石漠化坡地;地表水中的钙离子流失总量和地表径流量、土层厚度、岩石裸露率均有较高的相关性,其中与地表径流量达到显著性相关。

关 键 词:石漠化  钙离子  径流  粤北
收稿时间:2011-5-23
修稿时间:2011-7-11

Calcium Ion Loss along with Runoff on Shrub Slopes in Rock Desertification Area of Northern Guangdong under Rainfall Simulation Experiment
WEI Xing-hu,LU Guan-yao,ZHOU Hong-yan,XU Xi-zhen,LEI Li.Calcium Ion Loss along with Runoff on Shrub Slopes in Rock Desertification Area of Northern Guangdong under Rainfall Simulation Experiment[J].Journal of Desert Research,2011,31(5):1343-1347.
Authors:WEI Xing-hu  LU Guan-yao  ZHOU Hong-yan  XU Xi-zhen  LEI Li
Institution:WEI Xing-hu1,LU Guan-yao1,ZHOU Hong-yan2,XU Xi-zhen2,LEI Li2(1.Resources and Environmental Science Research Institute,Foshan University,Foshan 528000,Guangdong,China,2.School of Geography,South China Normal University,Guangzhou 510631,China)
Abstract:Calcium ion loss volumes with runoff for 30 minutes on shrub slopes in different rock desertification areas in northern Guangdong were observed in a rainfall simulation experiment.Results show that: under different simulated precipitation densities,the variation of runoff,calcium ion concentration and total calcium ion loss with runoff for 30 minutes over shrub slope in different degrees of rock desertification area like an inverted U type;under a specific rainfall intensity,the calcium ion loss on shrub sl...
Keywords:rock desertification  calcium ion  runoff  Northern Guangdong  
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